Abstract
The new biostratigraphyc data and the revision of the old data, suggest us to show for this one age Upper Cenomanien up to Middle Turonian. The distribution of the different sediments and the relations among the different Litostrati, graphic units, we can explain by the development of a Cycle. This Cycle is formed by one fast transgression of the open Shelf, followed by a progradation of the near Shelf. All of this evolution is in relation with too eustatic changos of the sea level.
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